Hauptseite > Publikationsdatenbank > Imaging water fluxes in porous media by magnetic resonance imaging using D2O as a tracer > print |
001 | 3486 | ||
005 | 20200423202449.0 | ||
024 | 7 | _ | |2 pmid |a pmid:18701229 |
024 | 7 | _ | |2 DOI |a 10.1016/j.mri.2008.06.007 |
024 | 7 | _ | |2 WOS |a WOS:000263533300015 |
037 | _ | _ | |a PreJuSER-3486 |
041 | _ | _ | |a eng |
082 | _ | _ | |a 610 |
084 | _ | _ | |2 WoS |a Radiology, Nuclear Medicine & Medical Imaging |
100 | 1 | _ | |a Pohlmeier, A. |b 0 |u FZJ |0 P:(DE-Juel1)VDB1270 |
245 | _ | _ | |a Imaging water fluxes in porous media by magnetic resonance imaging using D2O as a tracer |
260 | _ | _ | |a Amsterdam [u.a.] |b Elsevier Science |c 2009 |
300 | _ | _ | |a 285 - 292 |
336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |2 PUB:(DE-HGF) |
336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
336 | 7 | _ | |a ARTICLE |2 BibTeX |
336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
336 | 7 | _ | |a article |2 DRIVER |
440 | _ | 0 | |a Magnetic Resonance Imaging |x 0730-725X |0 4146 |y 2 |v 27 |
500 | _ | _ | |a Record converted from VDB: 12.11.2012 |
520 | _ | _ | |a In this study, we investigate the usefulness of D(2)O as a conservative tracer for monitoring water flux by MRI in a heterogeneous sand column. The column consisted of a cylindrical 3x9-cm packing of fine sand in which an 8-mm diameter cylindrical obstacle was placed. Constant steady-state flux densities between J(w)=0.07 and 0.28 cm min(-1) corresponding to mean pore flow velocities between 0.20 and 0.79 cm min(-1) were imposed at the top of the sand column, and a constant hydraulic head of -39 cm was maintained at the lower boundary. We injected pulses of 0.01 M NiCl(2) and 55% D(2)O and monitored the motion of the tracer plumes by MRI using a fast spin echo sequence over a period of 20 min. We observed that the center of gravity of all plumes moved with the mean pore flow velocity, which showed that D(2)O behaves as a conservative tracer. The motion of the tracer plume at J(w)=0.14 cm min(-1) was validated by a numerical simulation using HYDRUS2D, which reproduced the experimentally observed behavior very satisfactorily. |
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588 | _ | _ | |a Dataset connected to Web of Science, Pubmed |
650 | _ | 7 | |a J |2 WoSType |
653 | 2 | 0 | |2 Author |a MRI |
653 | 2 | 0 | |2 Author |a Sand |
653 | 2 | 0 | |2 Author |a Transport |
653 | 2 | 0 | |2 Author |a Flux |
653 | 2 | 0 | |2 Author |a Tracer |
653 | 2 | 0 | |2 Author |a Modeling |
653 | 2 | 0 | |2 Author |a HYDRUS2D |
700 | 1 | _ | |a van Dusschoten, D. |b 1 |u FZJ |0 P:(DE-Juel1)129425 |
700 | 1 | _ | |a Weihermüller, L. |b 2 |u FZJ |0 P:(DE-Juel1)VDB17057 |
700 | 1 | _ | |a Schurr, U. |b 3 |u FZJ |0 P:(DE-Juel1)129402 |
700 | 1 | _ | |a Vereecken, H. |b 4 |u FZJ |0 P:(DE-Juel1)129549 |
773 | _ | _ | |a 10.1016/j.mri.2008.06.007 |g Vol. 27, p. 285 - 292 |p 285 - 292 |q 27<285 - 292 |0 PERI:(DE-600)1500646-3 |t Magnetic resonance imaging |v 27 |y 2009 |x 0730-725X |
856 | 7 | _ | |u http://dx.doi.org/10.1016/j.mri.2008.06.007 |
856 | 4 | _ | |u https://juser.fz-juelich.de/record/3486/files/FZJ-3486.pdf |z Published final document. |y Restricted |
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914 | 1 | _ | |y 2009 |
915 | _ | _ | |0 StatID:(DE-HGF)0010 |a JCR/ISI refereed |
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920 | 1 | _ | |d 31.10.2010 |g ICG |k ICG-4 |l Agrosphäre |0 I:(DE-Juel1)VDB793 |x 2 |
920 | 1 | _ | |0 I:(DE-82)080011_20140620 |k JARA-ENERGY |l Jülich-Aachen Research Alliance - Energy |g JARA |x 3 |
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